Holocene vegetation changes through Lac Ledro sediments (Trentino, Italy).

Poster International audience Lake Ledro is part of the French program ANR LAMA (coordinators: M. Magny and N. Combourieu Nebout) which aims to link Holocene paleoenvironmental changes along a north-south transect in Italy. Lake Ledro (652 m a.s.l.; Trentino, north-eastern Italy) is the northward co...

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Main Authors: Joannin, Sébastien, Vannière, Boris, Galop, Didier, Magny, Michel, Gilli, Adrian, Chapron, Emmanuel, Wirth, Stefanie, Anselmetti, Flavio, Desmet, Marc
Other Authors: Laboratoire Chrono-environnement (UMR 6249) (LCE), Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC), Université Bourgogne Franche-Comté COMUE (UBFC)-Université Bourgogne Franche-Comté COMUE (UBFC), PaleoEnvironnements et PaleobioSphere (PEPS), Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Maison des Sciences de l'Homme et de l'Environnement Claude Nicolas Ledoux (UAR 3124) (MSHE), Géographie de l'environnement (GEODE), Université Toulouse - Jean Jaurès (UT2J), Université de Toulouse (UT)-Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS), Department of Earth Sciences Swiss Federal Institute of Technology - ETH Zürich (D-ERDW), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich), Institut des Sciences de la Terre d'Orléans (ISTO), Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Université de Tours (UT)-Centre National de la Recherche Scientifique (CNRS), Geological Institute ETH Zürich, Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)-Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich), ACCES-INRP
Format: Conference Object
Language:English
Published: HAL CCSD 2010
Subjects:
Online Access:https://hal.science/hal-00481825
id ftunifranchecom:oai:HAL:hal-00481825v1
record_format openpolar
institution Open Polar
collection Université de Franche-Comté (UFC): HAL
op_collection_id ftunifranchecom
language English
topic [SDE]Environmental Sciences
[SHS.ENVIR]Humanities and Social Sciences/Environmental studies
spellingShingle [SDE]Environmental Sciences
[SHS.ENVIR]Humanities and Social Sciences/Environmental studies
Joannin, Sébastien
Vannière, Boris
Galop, Didier
Magny, Michel
Gilli, Adrian
Chapron, Emmanuel
Wirth, Stefanie
Anselmetti, Flavio
Desmet, Marc
Holocene vegetation changes through Lac Ledro sediments (Trentino, Italy).
topic_facet [SDE]Environmental Sciences
[SHS.ENVIR]Humanities and Social Sciences/Environmental studies
description Poster International audience Lake Ledro is part of the French program ANR LAMA (coordinators: M. Magny and N. Combourieu Nebout) which aims to link Holocene paleoenvironmental changes along a north-south transect in Italy. Lake Ledro (652 m a.s.l.; Trentino, north-eastern Italy) is the northward component of the transect. It is located on the southern slope of the Alps and its catchment area covers 131 km2 with mountains culminating at 1500-2000 m. A multi-proxy approach based on biotic and abiotic indicators (lake-level, palynology, geochemistry and geophysic) was developed from deep and littoral cores, including sediment sequences in Early and Middle Bronze Age lake-shore archaeological sites. We aim reconstructing paleoenvironmental changes resulting from both climate and anthropic influences trough the entire Holocene. A deep master core was built after extracting twin cores from a non disturbed sediment zone recognised by seismic-reflexion investigations. The age-depth model is based on 13 AMS 14C ages measured on terrestrial plant macrofossils and the mean temporal resolution for analyses is ca 60 years. Palynological study shows the usual vegetation succession for the southern slope of the Alps. During the first part of the Holocene, abrupt changes are observed in pollen assemblages in relation to changes in other proxies (XRF and Magnetic Susceptibility) and correlate with cold events associated to the deglaciation in the North-Atlantic area. Cool episodes corresponding to the PreBoreal Oscillation (ca 11.3 ka cal BP) and 8.2 ka event are respectively characterized by stopping afforestation and a strong development of Abies in the local ecosystem. During the second part of the Holocene, two declines of arboreal pollen abundance are observed in relation with occurrences in both cereal and anthropic pollen indicators. These two phases are confirmed by increase in soil erosion as indicated by abiotic proxies. They give evidence of two successive steps for human settlement (Early-Middle Bronze Age and ...
author2 Laboratoire Chrono-environnement (UMR 6249) (LCE)
Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC)
Université Bourgogne Franche-Comté COMUE (UBFC)-Université Bourgogne Franche-Comté COMUE (UBFC)
PaleoEnvironnements et PaleobioSphere (PEPS)
Université Claude Bernard Lyon 1 (UCBL)
Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Maison des Sciences de l'Homme et de l'Environnement Claude Nicolas Ledoux (UAR 3124) (MSHE)
Géographie de l'environnement (GEODE)
Université Toulouse - Jean Jaurès (UT2J)
Université de Toulouse (UT)-Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS)
Department of Earth Sciences Swiss Federal Institute of Technology - ETH Zürich (D-ERDW)
Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)
Institut des Sciences de la Terre d'Orléans (ISTO)
Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Université de Tours (UT)-Centre National de la Recherche Scientifique (CNRS)
Geological Institute ETH Zürich
Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)-Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)
ACCES-INRP
format Conference Object
author Joannin, Sébastien
Vannière, Boris
Galop, Didier
Magny, Michel
Gilli, Adrian
Chapron, Emmanuel
Wirth, Stefanie
Anselmetti, Flavio
Desmet, Marc
author_facet Joannin, Sébastien
Vannière, Boris
Galop, Didier
Magny, Michel
Gilli, Adrian
Chapron, Emmanuel
Wirth, Stefanie
Anselmetti, Flavio
Desmet, Marc
author_sort Joannin, Sébastien
title Holocene vegetation changes through Lac Ledro sediments (Trentino, Italy).
title_short Holocene vegetation changes through Lac Ledro sediments (Trentino, Italy).
title_full Holocene vegetation changes through Lac Ledro sediments (Trentino, Italy).
title_fullStr Holocene vegetation changes through Lac Ledro sediments (Trentino, Italy).
title_full_unstemmed Holocene vegetation changes through Lac Ledro sediments (Trentino, Italy).
title_sort holocene vegetation changes through lac ledro sediments (trentino, italy).
publisher HAL CCSD
publishDate 2010
url https://hal.science/hal-00481825
op_coverage Vienne, Austria
genre North Atlantic
genre_facet North Atlantic
op_source EGU Natural and anthropogenic environmental change as evidenced in high-resolution continental archives (co-listed)
https://hal.science/hal-00481825
EGU Natural and anthropogenic environmental change as evidenced in high-resolution continental archives (co-listed), May 2010, Vienne, Austria
op_relation hal-00481825
https://hal.science/hal-00481825
_version_ 1810464583565967360
spelling ftunifranchecom:oai:HAL:hal-00481825v1 2024-09-15T18:24:15+00:00 Holocene vegetation changes through Lac Ledro sediments (Trentino, Italy). Joannin, Sébastien Vannière, Boris Galop, Didier Magny, Michel Gilli, Adrian Chapron, Emmanuel Wirth, Stefanie Anselmetti, Flavio Desmet, Marc Laboratoire Chrono-environnement (UMR 6249) (LCE) Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC) Université Bourgogne Franche-Comté COMUE (UBFC)-Université Bourgogne Franche-Comté COMUE (UBFC) PaleoEnvironnements et PaleobioSphere (PEPS) Université Claude Bernard Lyon 1 (UCBL) Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Maison des Sciences de l'Homme et de l'Environnement Claude Nicolas Ledoux (UAR 3124) (MSHE) Géographie de l'environnement (GEODE) Université Toulouse - Jean Jaurès (UT2J) Université de Toulouse (UT)-Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS) Department of Earth Sciences Swiss Federal Institute of Technology - ETH Zürich (D-ERDW) Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich) Institut des Sciences de la Terre d'Orléans (ISTO) Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Université de Tours (UT)-Centre National de la Recherche Scientifique (CNRS) Geological Institute ETH Zürich Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)-Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich) ACCES-INRP Vienne, Austria 2010-05-02 https://hal.science/hal-00481825 en eng HAL CCSD hal-00481825 https://hal.science/hal-00481825 EGU Natural and anthropogenic environmental change as evidenced in high-resolution continental archives (co-listed) https://hal.science/hal-00481825 EGU Natural and anthropogenic environmental change as evidenced in high-resolution continental archives (co-listed), May 2010, Vienne, Austria [SDE]Environmental Sciences [SHS.ENVIR]Humanities and Social Sciences/Environmental studies info:eu-repo/semantics/conferenceObject Conference papers 2010 ftunifranchecom 2024-07-01T23:39:52Z Poster International audience Lake Ledro is part of the French program ANR LAMA (coordinators: M. Magny and N. Combourieu Nebout) which aims to link Holocene paleoenvironmental changes along a north-south transect in Italy. Lake Ledro (652 m a.s.l.; Trentino, north-eastern Italy) is the northward component of the transect. It is located on the southern slope of the Alps and its catchment area covers 131 km2 with mountains culminating at 1500-2000 m. A multi-proxy approach based on biotic and abiotic indicators (lake-level, palynology, geochemistry and geophysic) was developed from deep and littoral cores, including sediment sequences in Early and Middle Bronze Age lake-shore archaeological sites. We aim reconstructing paleoenvironmental changes resulting from both climate and anthropic influences trough the entire Holocene. A deep master core was built after extracting twin cores from a non disturbed sediment zone recognised by seismic-reflexion investigations. The age-depth model is based on 13 AMS 14C ages measured on terrestrial plant macrofossils and the mean temporal resolution for analyses is ca 60 years. Palynological study shows the usual vegetation succession for the southern slope of the Alps. During the first part of the Holocene, abrupt changes are observed in pollen assemblages in relation to changes in other proxies (XRF and Magnetic Susceptibility) and correlate with cold events associated to the deglaciation in the North-Atlantic area. Cool episodes corresponding to the PreBoreal Oscillation (ca 11.3 ka cal BP) and 8.2 ka event are respectively characterized by stopping afforestation and a strong development of Abies in the local ecosystem. During the second part of the Holocene, two declines of arboreal pollen abundance are observed in relation with occurrences in both cereal and anthropic pollen indicators. These two phases are confirmed by increase in soil erosion as indicated by abiotic proxies. They give evidence of two successive steps for human settlement (Early-Middle Bronze Age and ... Conference Object North Atlantic Université de Franche-Comté (UFC): HAL